Improving groundwater storage change estimates using time-lapse gravimetry with Gravi4GW
Time-lapse gravimetry (repeat microgravity measurement) is a powerful tool for monitoring temporal mass distribution variations, including seasonal and long-term groundwater storage changes (GWSC). This geophysical method for measuring changes in gravity (Δg) is potentially applicable to any groundw...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Halloran, Landon J.S. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2022transfer abstract |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Long term evolution of Molniya orbit under the effect of Earth’s non-spherical gravitational perturbation - Zhu, Ting-Lei ELSEVIER, 2014, Amsterdam [u.a.] |
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| Übergeordnetes Werk: |
volume:150 ; year:2022 ; pages:0 |
| Links: |
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| DOI / URN: |
10.1016/j.envsoft.2022.105340 |
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| 520 | |a Time-lapse gravimetry (repeat microgravity measurement) is a powerful tool for monitoring temporal mass distribution variations, including seasonal and long-term groundwater storage changes (GWSC). This geophysical method for measuring changes in gravity (Δg) is potentially applicable to any groundwater system. Here, I present Gravi4GW, a Python tool for the site-adapted calculation of β, the conversion factor between Δg and GWSC (also known as "topographic admittance"). Alpine catchments, in particular, are ideal target sites as they are highly sensitive to climate variations and can experience significant GWSC, while often lacking groundwater monitoring infrastructure. Therefore, to illustrate the usage of Gravi4GW, I investigate a detailed example of an alpine catchment and examine spatial variations and the effects of depth assumptions. This novel and accessible tool is designed to be useful in both the planning and data processing stages of time-lapse gravimetric field studies. | ||
| 520 | |a Time-lapse gravimetry (repeat microgravity measurement) is a powerful tool for monitoring temporal mass distribution variations, including seasonal and long-term groundwater storage changes (GWSC). This geophysical method for measuring changes in gravity (Δg) is potentially applicable to any groundwater system. Here, I present Gravi4GW, a Python tool for the site-adapted calculation of β, the conversion factor between Δg and GWSC (also known as "topographic admittance"). Alpine catchments, in particular, are ideal target sites as they are highly sensitive to climate variations and can experience significant GWSC, while often lacking groundwater monitoring infrastructure. Therefore, to illustrate the usage of Gravi4GW, I investigate a detailed example of an alpine catchment and examine spatial variations and the effects of depth assumptions. This novel and accessible tool is designed to be useful in both the planning and data processing stages of time-lapse gravimetric field studies. | ||
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10.1016/j.envsoft.2022.105340 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001776.pica (DE-627)ELV057086753 (ELSEVIER)S1364-8152(22)00046-9 DE-627 ger DE-627 rakwb eng 520 VZ 620 VZ 610 570 VZ 44.89 bkl Halloran, Landon J.S. verfasserin aut Improving groundwater storage change estimates using time-lapse gravimetry with Gravi4GW 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Time-lapse gravimetry (repeat microgravity measurement) is a powerful tool for monitoring temporal mass distribution variations, including seasonal and long-term groundwater storage changes (GWSC). This geophysical method for measuring changes in gravity (Δg) is potentially applicable to any groundwater system. Here, I present Gravi4GW, a Python tool for the site-adapted calculation of β, the conversion factor between Δg and GWSC (also known as "topographic admittance"). Alpine catchments, in particular, are ideal target sites as they are highly sensitive to climate variations and can experience significant GWSC, while often lacking groundwater monitoring infrastructure. Therefore, to illustrate the usage of Gravi4GW, I investigate a detailed example of an alpine catchment and examine spatial variations and the effects of depth assumptions. This novel and accessible tool is designed to be useful in both the planning and data processing stages of time-lapse gravimetric field studies. Time-lapse gravimetry (repeat microgravity measurement) is a powerful tool for monitoring temporal mass distribution variations, including seasonal and long-term groundwater storage changes (GWSC). This geophysical method for measuring changes in gravity (Δg) is potentially applicable to any groundwater system. Here, I present Gravi4GW, a Python tool for the site-adapted calculation of β, the conversion factor between Δg and GWSC (also known as "topographic admittance"). Alpine catchments, in particular, are ideal target sites as they are highly sensitive to climate variations and can experience significant GWSC, while often lacking groundwater monitoring infrastructure. Therefore, to illustrate the usage of Gravi4GW, I investigate a detailed example of an alpine catchment and examine spatial variations and the effects of depth assumptions. This novel and accessible tool is designed to be useful in both the planning and data processing stages of time-lapse gravimetric field studies. Time-lapse gravimetry Elsevier Hydrogeophysics Elsevier Topographic admittance Elsevier Groundwater storage Elsevier Gravimetry Elsevier Alpine hydrology Elsevier Enthalten in Elsevier Science Zhu, Ting-Lei ELSEVIER Long term evolution of Molniya orbit under the effect of Earth’s non-spherical gravitational perturbation 2014 Amsterdam [u.a.] (DE-627)ELV017414318 volume:150 year:2022 pages:0 https://doi.org/10.1016/j.envsoft.2022.105340 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_70 44.89 Endokrinologie VZ AR 150 2022 0 |
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10.1016/j.envsoft.2022.105340 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001776.pica (DE-627)ELV057086753 (ELSEVIER)S1364-8152(22)00046-9 DE-627 ger DE-627 rakwb eng 520 VZ 620 VZ 610 570 VZ 44.89 bkl Halloran, Landon J.S. verfasserin aut Improving groundwater storage change estimates using time-lapse gravimetry with Gravi4GW 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Time-lapse gravimetry (repeat microgravity measurement) is a powerful tool for monitoring temporal mass distribution variations, including seasonal and long-term groundwater storage changes (GWSC). This geophysical method for measuring changes in gravity (Δg) is potentially applicable to any groundwater system. Here, I present Gravi4GW, a Python tool for the site-adapted calculation of β, the conversion factor between Δg and GWSC (also known as "topographic admittance"). Alpine catchments, in particular, are ideal target sites as they are highly sensitive to climate variations and can experience significant GWSC, while often lacking groundwater monitoring infrastructure. Therefore, to illustrate the usage of Gravi4GW, I investigate a detailed example of an alpine catchment and examine spatial variations and the effects of depth assumptions. This novel and accessible tool is designed to be useful in both the planning and data processing stages of time-lapse gravimetric field studies. Time-lapse gravimetry (repeat microgravity measurement) is a powerful tool for monitoring temporal mass distribution variations, including seasonal and long-term groundwater storage changes (GWSC). This geophysical method for measuring changes in gravity (Δg) is potentially applicable to any groundwater system. Here, I present Gravi4GW, a Python tool for the site-adapted calculation of β, the conversion factor between Δg and GWSC (also known as "topographic admittance"). Alpine catchments, in particular, are ideal target sites as they are highly sensitive to climate variations and can experience significant GWSC, while often lacking groundwater monitoring infrastructure. Therefore, to illustrate the usage of Gravi4GW, I investigate a detailed example of an alpine catchment and examine spatial variations and the effects of depth assumptions. This novel and accessible tool is designed to be useful in both the planning and data processing stages of time-lapse gravimetric field studies. Time-lapse gravimetry Elsevier Hydrogeophysics Elsevier Topographic admittance Elsevier Groundwater storage Elsevier Gravimetry Elsevier Alpine hydrology Elsevier Enthalten in Elsevier Science Zhu, Ting-Lei ELSEVIER Long term evolution of Molniya orbit under the effect of Earth’s non-spherical gravitational perturbation 2014 Amsterdam [u.a.] (DE-627)ELV017414318 volume:150 year:2022 pages:0 https://doi.org/10.1016/j.envsoft.2022.105340 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_70 44.89 Endokrinologie VZ AR 150 2022 0 |
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10.1016/j.envsoft.2022.105340 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001776.pica (DE-627)ELV057086753 (ELSEVIER)S1364-8152(22)00046-9 DE-627 ger DE-627 rakwb eng 520 VZ 620 VZ 610 570 VZ 44.89 bkl Halloran, Landon J.S. verfasserin aut Improving groundwater storage change estimates using time-lapse gravimetry with Gravi4GW 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Time-lapse gravimetry (repeat microgravity measurement) is a powerful tool for monitoring temporal mass distribution variations, including seasonal and long-term groundwater storage changes (GWSC). This geophysical method for measuring changes in gravity (Δg) is potentially applicable to any groundwater system. Here, I present Gravi4GW, a Python tool for the site-adapted calculation of β, the conversion factor between Δg and GWSC (also known as "topographic admittance"). Alpine catchments, in particular, are ideal target sites as they are highly sensitive to climate variations and can experience significant GWSC, while often lacking groundwater monitoring infrastructure. Therefore, to illustrate the usage of Gravi4GW, I investigate a detailed example of an alpine catchment and examine spatial variations and the effects of depth assumptions. This novel and accessible tool is designed to be useful in both the planning and data processing stages of time-lapse gravimetric field studies. Time-lapse gravimetry (repeat microgravity measurement) is a powerful tool for monitoring temporal mass distribution variations, including seasonal and long-term groundwater storage changes (GWSC). This geophysical method for measuring changes in gravity (Δg) is potentially applicable to any groundwater system. Here, I present Gravi4GW, a Python tool for the site-adapted calculation of β, the conversion factor between Δg and GWSC (also known as "topographic admittance"). Alpine catchments, in particular, are ideal target sites as they are highly sensitive to climate variations and can experience significant GWSC, while often lacking groundwater monitoring infrastructure. Therefore, to illustrate the usage of Gravi4GW, I investigate a detailed example of an alpine catchment and examine spatial variations and the effects of depth assumptions. This novel and accessible tool is designed to be useful in both the planning and data processing stages of time-lapse gravimetric field studies. Time-lapse gravimetry Elsevier Hydrogeophysics Elsevier Topographic admittance Elsevier Groundwater storage Elsevier Gravimetry Elsevier Alpine hydrology Elsevier Enthalten in Elsevier Science Zhu, Ting-Lei ELSEVIER Long term evolution of Molniya orbit under the effect of Earth’s non-spherical gravitational perturbation 2014 Amsterdam [u.a.] (DE-627)ELV017414318 volume:150 year:2022 pages:0 https://doi.org/10.1016/j.envsoft.2022.105340 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_70 44.89 Endokrinologie VZ AR 150 2022 0 |
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10.1016/j.envsoft.2022.105340 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001776.pica (DE-627)ELV057086753 (ELSEVIER)S1364-8152(22)00046-9 DE-627 ger DE-627 rakwb eng 520 VZ 620 VZ 610 570 VZ 44.89 bkl Halloran, Landon J.S. verfasserin aut Improving groundwater storage change estimates using time-lapse gravimetry with Gravi4GW 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Time-lapse gravimetry (repeat microgravity measurement) is a powerful tool for monitoring temporal mass distribution variations, including seasonal and long-term groundwater storage changes (GWSC). This geophysical method for measuring changes in gravity (Δg) is potentially applicable to any groundwater system. Here, I present Gravi4GW, a Python tool for the site-adapted calculation of β, the conversion factor between Δg and GWSC (also known as "topographic admittance"). Alpine catchments, in particular, are ideal target sites as they are highly sensitive to climate variations and can experience significant GWSC, while often lacking groundwater monitoring infrastructure. Therefore, to illustrate the usage of Gravi4GW, I investigate a detailed example of an alpine catchment and examine spatial variations and the effects of depth assumptions. This novel and accessible tool is designed to be useful in both the planning and data processing stages of time-lapse gravimetric field studies. Time-lapse gravimetry (repeat microgravity measurement) is a powerful tool for monitoring temporal mass distribution variations, including seasonal and long-term groundwater storage changes (GWSC). This geophysical method for measuring changes in gravity (Δg) is potentially applicable to any groundwater system. Here, I present Gravi4GW, a Python tool for the site-adapted calculation of β, the conversion factor between Δg and GWSC (also known as "topographic admittance"). Alpine catchments, in particular, are ideal target sites as they are highly sensitive to climate variations and can experience significant GWSC, while often lacking groundwater monitoring infrastructure. Therefore, to illustrate the usage of Gravi4GW, I investigate a detailed example of an alpine catchment and examine spatial variations and the effects of depth assumptions. This novel and accessible tool is designed to be useful in both the planning and data processing stages of time-lapse gravimetric field studies. Time-lapse gravimetry Elsevier Hydrogeophysics Elsevier Topographic admittance Elsevier Groundwater storage Elsevier Gravimetry Elsevier Alpine hydrology Elsevier Enthalten in Elsevier Science Zhu, Ting-Lei ELSEVIER Long term evolution of Molniya orbit under the effect of Earth’s non-spherical gravitational perturbation 2014 Amsterdam [u.a.] (DE-627)ELV017414318 volume:150 year:2022 pages:0 https://doi.org/10.1016/j.envsoft.2022.105340 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_70 44.89 Endokrinologie VZ AR 150 2022 0 |
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Halloran, Landon J.S. |
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Halloran, Landon J.S. ddc 520 ddc 620 ddc 610 bkl 44.89 Elsevier Time-lapse gravimetry Elsevier Hydrogeophysics Elsevier Topographic admittance Elsevier Groundwater storage Elsevier Gravimetry Elsevier Alpine hydrology Improving groundwater storage change estimates using time-lapse gravimetry with Gravi4GW |
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ddc 520 ddc 620 ddc 610 bkl 44.89 Elsevier Time-lapse gravimetry Elsevier Hydrogeophysics Elsevier Topographic admittance Elsevier Groundwater storage Elsevier Gravimetry Elsevier Alpine hydrology |
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ddc 520 ddc 620 ddc 610 bkl 44.89 Elsevier Time-lapse gravimetry Elsevier Hydrogeophysics Elsevier Topographic admittance Elsevier Groundwater storage Elsevier Gravimetry Elsevier Alpine hydrology |
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Long term evolution of Molniya orbit under the effect of Earth’s non-spherical gravitational perturbation |
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Long term evolution of Molniya orbit under the effect of Earth’s non-spherical gravitational perturbation |
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Improving groundwater storage change estimates using time-lapse gravimetry with Gravi4GW |
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Improving groundwater storage change estimates using time-lapse gravimetry with Gravi4GW |
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Long term evolution of Molniya orbit under the effect of Earth’s non-spherical gravitational perturbation |
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Long term evolution of Molniya orbit under the effect of Earth’s non-spherical gravitational perturbation |
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10.1016/j.envsoft.2022.105340 |
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improving groundwater storage change estimates using time-lapse gravimetry with gravi4gw |
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Improving groundwater storage change estimates using time-lapse gravimetry with Gravi4GW |
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Time-lapse gravimetry (repeat microgravity measurement) is a powerful tool for monitoring temporal mass distribution variations, including seasonal and long-term groundwater storage changes (GWSC). This geophysical method for measuring changes in gravity (Δg) is potentially applicable to any groundwater system. Here, I present Gravi4GW, a Python tool for the site-adapted calculation of β, the conversion factor between Δg and GWSC (also known as "topographic admittance"). Alpine catchments, in particular, are ideal target sites as they are highly sensitive to climate variations and can experience significant GWSC, while often lacking groundwater monitoring infrastructure. Therefore, to illustrate the usage of Gravi4GW, I investigate a detailed example of an alpine catchment and examine spatial variations and the effects of depth assumptions. This novel and accessible tool is designed to be useful in both the planning and data processing stages of time-lapse gravimetric field studies. |
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Time-lapse gravimetry (repeat microgravity measurement) is a powerful tool for monitoring temporal mass distribution variations, including seasonal and long-term groundwater storage changes (GWSC). This geophysical method for measuring changes in gravity (Δg) is potentially applicable to any groundwater system. Here, I present Gravi4GW, a Python tool for the site-adapted calculation of β, the conversion factor between Δg and GWSC (also known as "topographic admittance"). Alpine catchments, in particular, are ideal target sites as they are highly sensitive to climate variations and can experience significant GWSC, while often lacking groundwater monitoring infrastructure. Therefore, to illustrate the usage of Gravi4GW, I investigate a detailed example of an alpine catchment and examine spatial variations and the effects of depth assumptions. This novel and accessible tool is designed to be useful in both the planning and data processing stages of time-lapse gravimetric field studies. |
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Time-lapse gravimetry (repeat microgravity measurement) is a powerful tool for monitoring temporal mass distribution variations, including seasonal and long-term groundwater storage changes (GWSC). This geophysical method for measuring changes in gravity (Δg) is potentially applicable to any groundwater system. Here, I present Gravi4GW, a Python tool for the site-adapted calculation of β, the conversion factor between Δg and GWSC (also known as "topographic admittance"). Alpine catchments, in particular, are ideal target sites as they are highly sensitive to climate variations and can experience significant GWSC, while often lacking groundwater monitoring infrastructure. Therefore, to illustrate the usage of Gravi4GW, I investigate a detailed example of an alpine catchment and examine spatial variations and the effects of depth assumptions. This novel and accessible tool is designed to be useful in both the planning and data processing stages of time-lapse gravimetric field studies. |
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Improving groundwater storage change estimates using time-lapse gravimetry with Gravi4GW |
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